Dipole Tilt Effect on Magnetopause Reconnection and the Steady‐State Magnetosphere‐Ionosphere System: Global MHD Simulations

The Earth's dipole tilt angle changes both diurnally and seasonally and introduces numerous variabilities in the coupled magnetosphere‐ionosphere system. By altering the location and intensity of magnetic reconnection, the dipole tilt influences convection on a global scale. However, due to the...

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Veröffentlicht in:	Journal of geophysical research. Space physics 2020-07, Vol.125 (7), p.n/a
Hauptverfasser:	Eggington, J. W. B., Eastwood, J. P., Mejnertsen, L., Desai, R. T., Chittenden, J. P.
Format:	Artikel
Sprache:	eng
Schlagworte:	Attitude (inclination) Computational fluid dynamics Computer simulation Convection dipole tilt effects Dipoles Earth Earth magnetosphere field‐aligned currents Fluid flow Geomagnetic field global modeling Interplanetary magnetic field Ionosphere Magnetic fields Magnetic reconnection Magnetic separators Magnetohydrodynamics Magnetopause Magnetopause reconnection magnetosphere‐ionosphere coupling Magnetospheric convection Morphology Planetary orbits Polar caps Resistance Separators Simulation Solar magnetic field Solar storms Solar wind Space weather Upper atmosphere
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